TY - JOUR
T1 - The Regularized WSM6 Microphysical Scheme and Its Validation in WRF 4D-Var
AU - Yang, Sen
AU - Li, Deqin
AU - Chen, Liqiang
AU - Liu, Zhiquan
AU - Huang, Xiang Yu
AU - Pan, Xiao
N1 - Publisher Copyright:
© 2023, Institute of Atmospheric Physics/Chinese Academy of Sciences, and Science Press and Springer-Verlag GmbH Germany, part of Springer Nature.
PY - 2023/3
Y1 - 2023/3
N2 - A cold cloud assimilation scheme was developed that fully considers the water substances, i.e., water vapor, cloud water, rain, ice, snow, and graupel, based on the single-moment WSM6 microphysical scheme and four-dimensional variational (4D-Var) data assimilation in the Weather Research and Forecasting data assimilation (WRFDA) system. The verification of the regularized WSM6 and its tangent linearity model (TLM) and adjoint mode model (ADM) was proven successful. Two groups of single observation and real sounding data assimilation experiments were set up to further verify the correctness of the assimilation scheme. The results showed that the consideration of ice, snow, and graupel in the assimilation system of the 4D-Var, as opposed to their omission in the warm rain Kessler scheme, allowed the water substances to be reasonably updated, further improving the forecast. Before it can be further applied in the assimilation of observational data, radar reflectivities, and satellite radiances, the cold cloud assimilation scheme needs additional verification, including using conventional ground and sounding observations in the 4D-Var assimilation system.
AB - A cold cloud assimilation scheme was developed that fully considers the water substances, i.e., water vapor, cloud water, rain, ice, snow, and graupel, based on the single-moment WSM6 microphysical scheme and four-dimensional variational (4D-Var) data assimilation in the Weather Research and Forecasting data assimilation (WRFDA) system. The verification of the regularized WSM6 and its tangent linearity model (TLM) and adjoint mode model (ADM) was proven successful. Two groups of single observation and real sounding data assimilation experiments were set up to further verify the correctness of the assimilation scheme. The results showed that the consideration of ice, snow, and graupel in the assimilation system of the 4D-Var, as opposed to their omission in the warm rain Kessler scheme, allowed the water substances to be reasonably updated, further improving the forecast. Before it can be further applied in the assimilation of observational data, radar reflectivities, and satellite radiances, the cold cloud assimilation scheme needs additional verification, including using conventional ground and sounding observations in the 4D-Var assimilation system.
KW - 4D-Var
KW - data assimilation
KW - linearization
KW - numerical weather prediction
KW - WSM6
UR - https://www.scopus.com/pages/publications/85146558331
U2 - 10.1007/s00376-022-2058-6
DO - 10.1007/s00376-022-2058-6
M3 - Article
AN - SCOPUS:85146558331
SN - 0256-1530
VL - 40
SP - 483
EP - 500
JO - Advances in Atmospheric Sciences
JF - Advances in Atmospheric Sciences
IS - 3
ER -